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From rainfall to slope instability: an automatic GIS procedure for susceptibility analyses over wide areas.

机译:从降雨到边坡失稳:用于大范围敏感性分析的自动GIS程序。

摘要

The present paper proposes an automatic procedure in a GIS environment for the analysis and prediction of large-scale landslides due to rainfall events. It runs, for each unit cell, an hydrological balance based on the Curve Number method, CN (Soil Conservation Service 1972 and 1975), computing the evolution of groundwater as a result of precipitation and then checks the overcoming, or not, of limit equilibrium conditions of the land in the domain of interest. The mathematical model was implemented in the free and open source GIS GRASS. For any sequence of consecutive days of rain, according to the conditions of humidity prior to the time-history under study, the hydro-geotechnical model allows (1) the determination of the oscillations of the phreatic table, (2) the part of saturated soil and (3) the slope stability analysis, by taking into proper account the pore pressures build-up. The results of the procedure are returned in raster format, allowing an easy and intuitive interpretation of the land mass sensitivity to meteoric actions. This procedure was applied on an extensive kinematic phenomenon surrounding the city of Santo Stefano d'Aveto (Liguria, Italy). The realized maps of landslide susceptibility are in excellent agreement with what is evident on site.
机译:本文提出了一种在GIS环境下的自动程序,用于对降雨事件引起的大规模滑坡进行分析和预测。它为每个单位单元运行一个基于“曲线数”方法CN(水土保持服务1972和1975)的水文平衡,计算降水产生的地下水演化,然后检查是否克服了极限平衡利益范围内的土地条件。数学模型是在免费和开源的GIS GRASS中实现的。对于连续降雨的任何序列,根据研究的时间历程之前的湿度条件,水力岩土工程模型允许(1)确定潜水台的振动,(2)饱和部分土和(3)边坡稳定性分析,要适当考虑孔隙压力的增加。该过程的结果以栅格格式返回,从而可以轻松直观地解释陆地对流星活动的敏感性。此程序应用于围绕Santo Stefano d'Aveto(意大利利古里亚)的广泛运动学现象。所实现的滑坡敏感性图与现场明显吻合。

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